A meteorite is a natural object of extraterrestrial origin that survives passage through the atmosphere.

Pallasite

These are a unique structure of metal and gemstone. the asteroid was from between mars and Jupiter and is 4.6 billion years old.

This Jepra Pallasite was found in 2008 and The Meteoritical Society approved the jepra meteorite in July 2011.It consists of period ,olivines and is comprised of magnetite, nickel sulphide, sulphate and schreibersite.

A pallasite is of cosmic origin, that is a meteorite. But a meteorite, which brings the only known gems from the cosmos to the earth - also known as olivine or peridot. So many times less than the already rare meteorites.
This extremely rare and unusual pendant carries the force of the cosmos in himself, in the glass vial contains many fine Peridotedelsteine that originate from the asteroid belt, which are located in orbit between Mars and Jupiter..
The Jepara pallasite was found in 2008 on the island of Java in Indonesia. It consists of one piece and has a weight of 499.5 kg.

Silicate Iron Meteorites

Silicate irons consist of a great proportion of inclusions and the metal pattern within and it is usually consists of veins and clumps as well as, other material. They are quite lighter than pure Irons, and since these set of materials have varying burn features, the texture of the surface is more remarkable, with additional thumbprints, bowl-shaped depressions, which is similar with hollows or craters.

Stony-Iron Meteorites

Stony-Irons are exceptional and they are considered as the most attractive and valuable meteorites. It is indistinguishable when a silicate iron converts into a Stony-Iron. In fact, there are two types of meteorites: the pallasites and mesosiderites.

Mesosiderites are a collection of mineral and metal, meanwhile pallasites is the most attractive meteorite that is available nowadays, with big rocks of olivine, a yellow-green igneous stone, transparent in thin slices, or refined tones.

Stone Meteorites

Stone meteorites are considered as the most common form, but also the most valuable type because they are tough to differentiate from Earth rocks. They also grind down more rapidly than the robust stony-irons. Though these are the most diverse in composition and substance, they are separated into two different types,achondrites and chondrites.

Chondrites composed of chondrules, atomic to marble-sized, sphere-shaped globs of silicates from the most primitive solar-nebula, occasionally pre-dating yet, in planetary structure! This material is accreted into planetesimals, which were showered by other bodies, which results in the division and ruin of the planetesimal.

If the parent planetesimal expanded enough, the force and heat dissolved are re-crystallized into chondritic substance, which results intoachondrites, and the rarest structure of meteorite. Achondritic meteorites can be several pieces of other full-grown moons or planets, which were expelled by a huge impact